三种土壤质地工程堆积体坡面流速及产沙特征

李建明, 王一峰, 张长伟, 王文龙, 黄金权, 王志刚, 张冠华, 白芸

长江科学院院报 ›› 2019, Vol. 36 ›› Issue (12) : 28-35.

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长江科学院院报 ›› 2019, Vol. 36 ›› Issue (12) : 28-35. DOI: 10.11988/ckyyb.20190134
水土保持与生态建设

三种土壤质地工程堆积体坡面流速及产沙特征

  • 李建明1,2,3, 王一峰1, 张长伟1, 王文龙2,4, 黄金权1, 王志刚1, 张冠华1, 白芸5
作者信息 +

Characteristic of Flow Velocity and Sediment Yielding on Engineering Accumulations Slope with Three Soil Textures

  • LI Jian-ming1,2,3, WANG Yi-feng1, ZHANG Chang-wei1, WANG Wen-long2,4, HUANG Jin-quan1,
    WANG Zhi-gang1, ZHANG Guan-hua1, BAI Yun5
Author information +
文章历史 +

摘要

生产建设项目工程堆积体由于土壤质地、砾石质量分数差异较大,导致侵蚀过程流速及产沙特性发生变化。通过人工模拟降雨试验,研究砂土、壤土及黏土3种土壤质地堆积体的流速与产沙特性。结果表明:①堆积体坡面流速在产流开始3 min内递增,随后趋于稳定;②小雨强时砂土堆积体侵蚀主要发生在产流的中后期,壤土堆积体发生在产流前期和中期,而黏土堆积体的侵蚀发生在整个降雨过程,21 min后的累计产沙量占次降雨总产沙量砂土、壤土和黏土堆积体分别为52.3%~95.6%、29.6%~44.9%和42.1%~50.0%;③产流历时、雨强与径流率、入渗率、流速、产沙率均呈显著相关性;④雨强增加1.5~2.0倍,3种土质堆积体侵蚀量增大1.2~39.8倍。相同雨强下砂土堆积体侵蚀量是壤土的6.0~6.3倍,是黏土的3.2~3.5倍;相同砾石质量分数下砂土堆积体侵蚀量分别是壤土和黏土的5.0~9.8倍和2.7~3.8倍。研究成果对于明确含砾石堆积体侵蚀过程机理具有重要意义,并为建立堆积体侵蚀预报模型奠定基础。

Abstract

The process of velocity and sediment yielding on engineering accumulations slope are different from traditional due to differences in soil textures and mass fraction of gravel in production and construction projects. In this paper we examined the characteristic of flow velocity and sediment yielding on engineering accumulations with three soil textures (sandy soil, loam, and clay) via artificial simulation experiments. Results showed that: (1) Flow velocity increased at first within 3 minutes after the beginning of the runoff and then stabilized. (2) For sandy soil accumulations,erosion mainly occurred in the middle and late stages of runoff at small rainfall intensity; for loam, in the early and middle stages; and for clay accumulations, throughout the whole runoff process. The accumulative sediment yielding 21 minutes after runoff beginning accounted for 52.3%-95.6%,29.6%-44.9%, and 42.1%-50.0% of the total erosion amount of sand, loam and clay accumulations. (3) Significant correlations were found with runoff rate, infiltration rate, velocity, and sediment yielding rate against runoff time and rainfall intensity. Erosion amount increased by 1.2-39.8 times as rainfall intensity increased 1.5-2.0 times. Erosion amount for sandy accumulations was 6.0-6.3 times that of loam accumulations, 3.2-3.5 times that of clay accumulations under the same rainfall intensity, and 5.0-9.8 times and 2.7-3.8 times those of loam and clay accumulations with the same mass fraction of gravel. The research findings are of great significance for clarifying the mechanism of erosion process of engineering accumulations, and lay a foundation for establishing the erosion prediction model for engineering accumulations.

关键词

工程堆积体 / 产沙 / 流速 / 砾石质量分数 / 土壤质地

Key words

engineering accumulations / sediment yielding / flow velocity / mass fraction of gravel / soil textures

引用本文

导出引用
李建明, 王一峰, 张长伟, 王文龙, 黄金权, 王志刚, 张冠华, 白芸. 三种土壤质地工程堆积体坡面流速及产沙特征[J]. 长江科学院院报. 2019, 36(12): 28-35 https://doi.org/10.11988/ckyyb.20190134
LI Jian-ming, WANG Yi-feng, ZHANG Chang-wei, WANG Wen-long, HUANG Jin-quan,
WANG Zhi-gang, ZHANG Guan-hua, BAI Yun.
Characteristic of Flow Velocity and Sediment Yielding on Engineering Accumulations Slope with Three Soil Textures[J]. Journal of Changjiang River Scientific Research Institute. 2019, 36(12): 28-35 https://doi.org/10.11988/ckyyb.20190134
中图分类号: S157.1   

参考文献

[1] LV J R, LUO H, XIE Y S. Effects of Rock Fragment Content, Size and Cover on Soil Erosion Dynamics of Spoil Heaps through Multiple Rainfall Events[J] . Catena, 2019, 172: 179-189.
[2] 张平仓, 周 若, 程冬兵, 等. 工程开挖面特征及土壤流失量快速监测方法探讨[J] .长江科学院院报,2013,30(9):22-26.
[3] WANG X Y, LI Z X, CAI C F, et al. Effects of Rock Fragment Cover on Hydrological Response and Soil Loss from Regosols in a Semi-humid Environment in South-West China[J] . Geomorphology, 2012, 151/152: 234-242.
[4] 倪含斌, 张丽萍. 神东矿区堆积弃土坡地入渗规律试验研究[J] .水土保持学报, 2007, 21(3):28-31.
[5] 郭朝旭. 松散滑坡堆积体降雨入渗过程的实验研究[R] .北京:中国地理学会,2013.
[6] 周蓓蓓, 邵明安, 王全九.不同碎石种类对土壤入渗的影响[J] .西北农林科技大学学报(自然科学版), 2011,39(10):141-147.
[7] 王慧芳, 邵明安.含碎石土壤水分入渗试验研究[J] .水科学进展, 2006, 17(5):604-609.
[8] 符素华.土壤中砾石存在对入渗影响研究进展[J] .水土保持学报, 2005, 1(1):171-175.
[9] 戎玉博,王森,白玉洁,等.含砾石锥状工程堆积体侵蚀水动力学特性和细沟形态特征[J] .水土保持学报,2018,32(2):134-141.
[10] 康宏亮,王文龙,薛智德,等.北方风沙区砾石对堆积体坡面径流及侵蚀特征的影响[J] .农业工程学报,2016,32(3):125-134.
[11] 朱 波, 莫 斌, 王 涛, 等. 紫色丘陵区工程建设松散堆积物的侵蚀研究[J] .水土保持学报, 2005,19(4): 193-195.
[12] 崔 斌, 苏芳莉, 郭成久. 模拟降雨条件下不同颗粒级配工程弃土的侵蚀实验[J] .中国水土保持科学, 2012, 10(2):61-65.
[13] 宓永宁,娄宗科. 建筑材料[M] .北京: 中国农业出版社,2006: 73-76.
[14] 张婧媛,张平仓,丁文峰.黄土与紫色土坡面侵蚀特征对比试验研究[J] .水土保持通报,2010,30(4):60-62,67.
[15] 史东梅,蒋光毅,彭旭东,等. 不同土石比的工程堆积体边坡径流侵蚀过程[J] . 农业工程学报,2015,31(17):152-161.
[16] POESEN J, LUNA E D, FRANCA A, et al. Concentrated Flow Erosion Rates as Affected by Rock Fragment Cover and Initial Soil Moisture Content[J] . Catena, 1999, 36: 319-325.
[17] 王小燕, 李朝霞, 徐勤学, 等. 砾石覆盖对土壤水蚀过程影响的研究进展[J] . 中国水土保持科学, 2011, 9(1): 115-120.
[18] 朱兴华,庄建琦,李亚哲,等.弃渣型泥石流输沙速率模型试验研究[J] .长江科学院院报,2017,34(9):41-46.
[19] 朱元骏, 邵明安. 不同碎石含量的土壤降雨入渗和产沙过程初步研究[J] . 农业工程学报, 2006, 22(2):64-67.
[20] 张冠华,程冬兵,张平仓,等.工程开挖面水土流失特征试验研究[J] .长江科学院院报,2015,32(3):27-30.
[21] IQBAL J, DAI F C, HONG M, et al. Failure Mechanism and Stability Analysis of an Active Landslide in the Xiangjiaba Reservoir Area, Southwest China[J] . Journal of Earth Science,2018, 29(3): 646-661.
[22] 唐 扬,殷坤龙,汪 洋,等. 斜坡降雨入渗的改进Mein-Larson模型[J] .地球科学,2017,42(4):634-640.
[23] 赵 暄,谢永生,景民晓,等.生产建设项目弃土堆置体下垫面仿真模拟标准化参数[J] .水土保持学报,2012,26(5):229-234.
[24] 雷廷武, 张晴雯, 闫丽娟. 细沟侵蚀物理模型[M] . 北京: 科学出版社, 2009:117-129.
[25] ALMEIDA W S, PANACHUKI E, OLIVEIRA P T S, et al. Effect of Soil Tillage and Vegetal Cover on Soil Water Infiltration[J] . Soil & Tillage Research, 2018,175: 130-138.
[26] ZHANG W, WEI C, LI Y, et al. Effects of Rock Fragments on Infiltration and Evaporation in Hilly Purple Soils of Sichuan Basin, China[J] . Environmental Earth Sciences, 2011, 62(8): 1655-1665.
[27] FIGUEIREDO T, POESEN J. Effects of Surface Rock Fragment Characteristics on Interrill Runoff and Erosion of a Silty Loam Soil[J] . Soil & Tillage Research, 1998, 46(1/2):81-95.
[28] PENG X D, SHI D M, JIANG D, et al. Runoff Erosion Process on Different Underlying Surfaces from Disturbed Soils in the Three Gorges Reservoir Area, China[J] . Catena, 2014, 123: 215-224.
[29] 李君兰,蔡强国,孙莉英,等. 坡面水流速度与坡面含砂量的关系[J] . 农业工程学报,2011,27(3):73-78.

基金

国家自然科学基金项目(41701316,41877082,41761062);国家重点研发计划重点专项(YS2016YFSF030019);水利部技术示范项目(SF201806);长江科学院中央级公益性科研院所基本科研业务费(CKSF2019179/TB,CKSF2019176/TB,CKSF2019248/TB)

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